Soil Data Explorer - STEINAUER

Official Series Description

Lab Data Summary

Aggregate lab data for the STEINAUER soil series. This aggregation is based on all pedons with a current taxon name of STEINAUER, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to STEINAUER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
102C	40A2180	S1968NE027003	Steinauer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.6552696,-97.4106293
106	03N0989	03NE109003	Steinauer	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6945572,-96.8560257
106	07KS005502	07KS005502	Steinauer	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.4296112,-95.3421936
106	07KS005503	07KS005503	Steinauer	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5615273,-95.4262466
106	96P0228	96NE159004	Steinauer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8294449,-96.9652786
106	40A2178	S1968NE133001	STEINAUER	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2188873,-96.2288895
106	40A2179	S1968NE133002	STEINAUER	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1991653,-96.2200012
107A	84P0773	84IA035004	Steinauer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.8666649,-95.6666641
107B	87P0326	87IA0090033	Steinauer	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.622776,-94.9552765
107B	04N0909	S2004NE055124	Steinauer	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3262367,-96.066864

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STEINAUER soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the STEINAUER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the STEINAUER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the STEINAUER series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

Competing Series

Soil series competing with STEINAUER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the STEINAUER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the STEINAUER series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with STEINAUER, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. KS-2012-01-20-03 | Atchison County - February 1984

   Typical pattern of soils in the Sharpsburg-Shelby association (Soil Survey of Atchison County, Kansas; 1984).

2. KS-2012-01-20-08 | Brown County - September 1960

   Typical cross section of the smooth, sloping, loess-till uplands (Soil Survey of Brown County, Kansas; 1960).

3. NE-2012-02-08-16 | Butler County - February 1982

   Typical pattern of soils in the Sharpsburg-Steinauer-Pawnee association and relationship of the soils to topography and parent material (Soil Survey of Butler County, Nebraska; February 1982).

4. NE-2012-02-08-17 | Gage County - May 1964

   Schematic diagram showing the relationship of major soil series to parent materials in Gage County, Nebraska (Soil Survey of Gage County, Nebraska; May 1964).

5. NE-2012-02-13-90 | Saunders County - January 1965

   Soils in the Burchard-Shelby association (Soil Survey of Saunders County, Nebraska; January 1965).

6. NE-2012-02-13-91 | Saunders County - January 1965

   Soils in the Monona association (Soil Survey of Saunders County, Nebraska; January 1965).

Map Units

Map units containing STEINAUER as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Steinauer clay loam, 25 to 40 percent slopes	33G	5755	403931	fkb1	ia035	1987	1:15840
Steinauer clay loam, 14 to 25 percent slopes	33F	1868	403930	fkb0	ia035	1987	1:15840
Steinauer-Steinauer variant clay loams, 20 to 50 percent slopes	633G	1364	403948	fkbl	ia035	1987	1:15840
Steinauer clay loam, 9 to 14 percent slopes	33D	1145	403929	fk9z	ia035	1987	1:15840
Steinauer-Hawick complex, 25 to 40 percent slopes	739G	967	403951	fkbp	ia035	1987	1:15840
Steinauer loam, 18 to 25 percent slopes	33F	251	406134	fmm3	ia071	1968	1:20000
Steinauer clay loam, 14 to 18 percent slopes, severely eroded	33E3	579	406763	fn8d	ia085	1971	1:15840
Steinauer clay loam, 9 to 14 percent slopes, moderately eroded	33D2	446	406762	fn8c	ia085	1971	1:15840
Steinauer-Burchard complex, 18 to 40 percent slopes	35G	569	407151	fnnx	ia093	1989	1:15840
Steinauer-Burchard complex, 14 to 18 percent slopes, moderately eroded	35E2	404	407149	fnnv	ia093	1989	1:15840
Steinauer clay loam, 25 to 40 percent slopes	33G	3286	409105	fqpy	ia119	1973	1:15840
Steinauer clay loam, 18 to 25 percent slopes	33F	2678	409104	fqpx	ia119	1973	1:15840
Steinauer clay loam, 14 to 18 percent slopes	33E	1399	409103	fqpw	ia119	1973	1:15840
Steinauer clay loam, 9 to 14 percent slopes	33D	1260	409102	fqpv	ia119	1973	1:15840
Steinauer clay loam, 5 to 9 percent slopes	33C	1005	409101	fqpt	ia119	1973	1:15840
Steinauer clay loam, 11 to 18 percent slopes	33D	310	409564	fr5r	ia129	1979	1:15840
Steinauer clay loam, 18 to 25 percent slopes	33F	293	447320	h0gp	ia133	1994	1:12000
Steinauer clay loam, 25 to 40 percent slopes	33G	210	447321	h0gq	ia133	1994	1:12000
Steinauer clay loam, 14 to 18 percent slopes	33E	167	447318	h0gm	ia133	1994	1:12000
Steinauer clay loam, 9 to 14 percent slopes	33D	16	447316	h0gk	ia133	1994	1:12000
Steinauer clay loam, 14 to 18 percent slopes, moderately eroded	33E2	674	409859	frh8	ia137	1987	1:15840
Steinauer clay loam, 9 to 14 percent slopes, moderately eroded	33D2	654	409858	frh7	ia137	1987	1:15840
Steinauer clay loam, 9 to 14 percent slopes, severely eroded	33D3	708	410344	frzx	ia149	1972	1:20000
Steinauer clay loam, 14 to 18 percent slopes, severely eroded	33E3	352	410345	frzy	ia149	1972	1:20000
Steinauer clay loam, 18 to 30 percent slopes, severely eroded	33F3	186	410346	frzz	ia149	1972	1:20000
Steinauer clay loam, 9 to 14 percent slopes, moderately eroded	33D2	808	410476	fs45	ia155	1986	1:15840
Steinauer clay loam, 14 to 18 percent slopes, moderately eroded	33E2	740	410477	fs46	ia155	1986	1:15840
Steinauer loam, 18 to 40 percent slopes	33F	381	410800	fsgm	ia161	1975	1:15840
Steinauer loam, 9 to 18 percent slopes	33E	155	410799	fsgl	ia161	1975	1:15840
Steinauer clay loam, 18 to 40 percent slopes	33G	2486	411223	fsx8	ia167	1987	1:15840
Steinauer clay loam, 9 to 14 percent slopes, moderately eroded	33D2	648	411221	fsx6	ia167	1987	1:15840
Steinauer clay loam, 14 to 18 percent slopes, moderately eroded	33E2	642	411222	fsx7	ia167	1987	1:15840
Steinauer clay loam, 5 to 9 percent slopes, moderately eroded	33C2	318	411220	fsx5	ia167	1987	1:15840
Shelby-Steinauer loams, 12 to 25 percent slopes	7594	5042	1475373	2v8zb	ks005	1998	1:24000
Burchard-Steinauer clay loams, 12 to 18 percent slopes	7225	1629	1152167	2qsk2	ks013	1994	1:24000
Burchard-Steinauer clay loams, 6 to 12 percent slopes	7224	1420	1480344	2qsk1	ks085	1976	1:24000
Burchard-Steinauer clay loams, 12 to 18 percent slopes	7225	133	1480345	2qsk2	ks085	1976	1:24000
Steinauer clay loam, 12 to 25 percent slopes	7608	75	1480368	2yrw3	ks085	1976	1:24000
Shelby-Steinauer loams, 12 to 25 percent slopes	7594	38	1480366	2v8zb	ks085	1976	1:24000
Steinauer-Shelby clay loams, 10 to 14 percent slopes	7609	5579	1457091	2yrw4	ks117	1977	1:24000
Steinauer clay loam, 12 to 25 percent slopes	7608	2055	1457090	2yrw3	ks117	1977	1:24000
Burchard-Steinauer clay loams, 6 to 12 percent slopes	7224	1151	1457080	2qsk1	ks117	1977	1:24000
Burchard-Steinauer clay loams, 6 to 12 percent slopes	7224	99765	1406018	2qsk1	ks131	1980	1:24000
Steinauer clay loam, 12 to 25 percent slopes	7608	3874	1406032	2yrw3	ks131	1980	1:24000
Burchard-Steinauer clay loams, 12 to 18 percent slopes	7225	9	1406019	2qsk2	ks131	1980	1:24000
Steinauer-Shelby clay loams, 10 to 14 percent slopes	7609	73	1480726	2yrw4	ks149	1984	1:24000
Burchard-Steinauer clay loams, 6 to 12 percent slopes	7224	56	1480713	2qsk1	ks149	1984	1:24000
Steinauer clay loam, 11 to 30 percent slopes, eroded	7612	4647	427863	gc71	ne021	1978	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	213	2216682	2ddmw	ne021	1978	1:20000
Steinauer soils, 11 to 30 percent slopes	7618	4	2216693	2ddn7	ne021	1978	1:20000
Steinauer clay loam, 11 to 30 percent slopes	7611	3637	1691327	2x6bs	ne023	1979	1:20000
Steinauer clay loam, 30 to 50 percent slopes	7619	2581	1691328	2yrwc	ne023	1979	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	2207	1691269	2v8y4	ne023	1979	1:20000
Steinauer clay loam, 6 to 11 percent slopes, eroded	7614	852	1691326	2yrw8	ne023	1979	1:20000
Ida-Steinauer complex, 17 to 60 percent slopes	8013	215	2219049	2dh37	ne023	1979	1:20000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	40	2219041	2v8y6	ne023	1979	1:20000
Ida-Steinauer complex, 17 to 60 percent slopes	8013	50	2216030	2dcyv	ne025	1981	1:20000
Steinauer clay loam, 11 to 30 percent slopes, eroded	7612	1745	427917	gc8s	ne037	1980	1:20000
Steinauer clay loam, 6 to 11 percent slopes, eroded	7614	696	427916	gc8r	ne037	1980	1:20000
Steinauer clay loam, 11 to 30 percent slopes, eroded	7612	461	426913	gb7d	ne053	1975	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	8	2217091	2df22	ne053	1975	1:20000
Ida-Steinauer complex, 17 to 60 percent slopes	8013	4	2217104	2df2h	ne053	1975	1:20000
Burchard-Contrary-Steinauer complex, 7 to 16 percent slopes	7210	326	1710933	2v8xp	ne055	2007	1:12000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	8822	1691092	2v8y6	ne067	2000	1:12000
Steinauer clay loam, 11 to 30 percent slopes	7611	4957	1691121	2x6bs	ne067	2000	1:12000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	4102	1691093	2v8y4	ne067	2000	1:12000
Steinauer clay loam, 30 to 50 percent slopes	7619	872	1691122	2yrwc	ne067	2000	1:12000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	63	2219198	2v8y6	ne095	1970	1:20000
Burchard-Steinauer clay loams, 11 to 30 percent slopes	7267	49	2219208	2v8y5	ne095	1970	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	25	2219197	2v8y4	ne095	1970	1:20000
Steinauer clay loam, 11 to 30 percent slopes	7611	13	2219202	2x6bs	ne095	1970	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	9071	1691570	2v8y4	ne097	1984	1:20000
Steinauer clay loam, 11 to 20 percent slopes	7610	722	1691597	2yrw5	ne097	1984	1:20000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	122	2219360	2v8y6	ne097	1984	1:20000
Steinauer clay loam, 11 to 30 percent slopes	7611	4	2219367	2x6bs	ne097	1984	1:20000
Steinauer loam, 11 to 30 percent slopes	7617	5765	1691390	2yrwb	ne109	1977	1:20000
Steinauer clay loam, 6 to 11 percent slopes, eroded	7614	3347	1691391	2yrw8	ne109	1977	1:20000
Steinauer clay loam, 20 to 40 percent slopes	7620	2167	1691392	2yrwd	ne109	1977	1:20000
Steinauer loam, 6 to 11 percent slopes	7616	1363	1691389	2yrw9	ne109	1977	1:20000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	153	2219240	2v8y6	ne109	1977	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	77	2219234	2v8y4	ne109	1977	1:20000
Ida-Steinauer complex, 17 to 60 percent slopes	8013	55	2219246	2dh9l	ne109	1977	1:20000
Burchard-Steinauer clay loams, 11 to 30 percent slopes	7267	36	2219235	2v8y5	ne109	1977	1:20000
Steinauer clay loam, 11 to 30 percent slopes	7611	8	2219236	2x6bs	ne109	1977	1:20000
Steinauer clay loam, 11 to 20 percent slopes	7610	1057	1691562	2yrw5	ne131	1979	1:20000
Steinauer clay loam, 11 to 20 percent slopes	7610	5372	1691640	2yrw5	ne133	1969	1:15840
Steinauer clay loam, 30 to 50 percent slopes	7619	4669	1691636	2yrwc	ne133	1969	1:15840
Steinauer clay loam, 6 to 11 percent slopes	7613	2838	1691639	2yrw7	ne133	1969	1:15840
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	233	2219389	2v8y4	ne133	1969	1:15840
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	102	2219390	2v8y6	ne133	1969	1:15840
Burchard-Steinauer clay loams, 11 to 30 percent slopes	7267	1135	1691139	2v8y5	ne151	1985	1:20000
Burchard-Contrary-Steinauer complex, 7 to 16 percent slopes	7210	144	1710997	2v8xp	ne153	2007	1:12000
Ida-Steinauer complex, 17 to 60 percent slopes	8013	6839	1691423	1ts21	ne155	1995	1:12000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	5484	1691415	2v8y4	ne155	1995	1:12000
Burchard-Steinauer clay loams, 6 to 11 percent slopes, eroded	7268	4222	1691414	2v8y6	ne155	1995	1:12000
Steinauer clay loam, 11 to 30 percent slopes	7611	1600	1691448	2x6bs	ne155	1995	1:12000
Steinauer clay loam, 20 to 40 percent slopes	7620	4	2219271	2yrwd	ne155	1995	1:12000
Steinauer clay loam, 11 to 30 percent slopes	7611	4733	1691249	2x6bs	ne159	1967	1:20000
Steinauer clay loam, 6 to 11 percent slopes, eroded	7614	3797	1691248	2yrw8	ne159	1967	1:20000
Steinauer clay loam, 30 to 50 percent slopes	7619	2959	1691239	2yrwc	ne159	1967	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes	7265	2394	1691195	2v8yg	ne159	1967	1:20000
Steinauer clay loam, 11 to 30 percent slopes, eroded	7612	1388	1691250	2yrw6	ne159	1967	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	597	1691196	2v8y4	ne159	1967	1:20000
Burchard-Steinauer clay loams, 11 to 30 percent slopes	7267	129	2219148	2v8y5	ne159	1967	1:20000
Steinauer loam, 11 to 30 percent slopes	7617	49	2219129	2yrwb	ne159	1967	1:20000
Steinauer clay loam, 20 to 40 percent slopes	7620	27	2219130	2yrwd	ne159	1967	1:20000
Steinauer soils, 11 to 30 percent slopes	7618	780	427748	gc3b	ne173	1966	1:20000
Steinauer clay loam, 11 to 30 percent slopes, eroded	7612	39	2217293	2df8l	ne173	1966	1:20000
Burchard-Steinauer clay loams, 11 to 17 percent slopes, eroded	7266	5445	395529	f8l0	ne177	2000	1:12000
Burchard-Contrary-Steinauer complex, 7 to 16 percent slopes	7210	8	2217302	2v8xp	ne177	2000	1:12000
Steinauer-Shindler clay loams, 24 to 40 percent slopes	SuF	2902	416659	fzkm	sd083	1971	1:20000
Steinauer-Shindler clay loams, 25 to 60 percent slopes	SsF	2374	446078	gz5m	sd099	1995	1:24000

Map of Series Extent

Approximate geographic distribution of the STEINAUER soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2024-10-30).